Preprints
https://doi.org/10.5194/egusphere-2024-641
https://doi.org/10.5194/egusphere-2024-641
14 Mar 2024
 | 14 Mar 2024

Interannual Variations of Terrestrial Water Storage in the East African Rift Region

Eva Boergens, Andreas Güntner, Mike Sips, Christian Schwatke, and Henryk Dobslaw

Abstract. The US-German GRACE (Gravity Recovery and Climate Experiment, 2002–2017) and GRACE-FO (GRACE-Follow-On, since 2018) satellite missions observe terrestrial water storage (TWS) variations. Over twenty years of data allow for investigating interannual variations beyond linear trends and seasonal signals. However, the origin of observed TWS changes, whether naturally caused or anthropogenic, cannot be determined solely with GRACE and GRACE-FO observations. This study focuses on the East African Rift region region around lakes Turkana, Victoria, and Tanganyika. It aims to characterise and analyse the interannual TWS variations together with surface water and meteorological observations and determine whether natural variability or human interventions caused these changes.

To this end, we apply the STL method (Seasonal Trend decomposition based on Loess) to separate the TWS signals into a seasonal signal, an interannual trend signal, and residuals. By clustering these interannual TWS dynamics for the African continent, we define the exact outline of the study's region.

In this area, a TWS decrease until 2006 was followed by a steady increase until around 2016, and Africa's most significant TWS increase occurred in 2019 and 2020. We found that besides precipitation and evaporation variability, surface water storage variations in the large lakes of the region explain large parts of the TWS variability. Storage dynamics of Lake Victoria regulated by the Nalubaale Dam alone contribute up to 50 % of the TWS changes. Satellite altimetry reveals the anthropogenically altered discharge downstream of the dam. It thus indicates that human intervention in the form of dam management at Lake Victoria substantially contributes to the TWS variability seen in the East African Rift region.

Publisher's note: Copernicus Publications remains neutral with regard to jurisdictional claims made in the text, published maps, institutional affiliations, or any other geographical representation in this preprint. The responsibility to include appropriate place names lies with the authors.
Eva Boergens, Andreas Güntner, Mike Sips, Christian Schwatke, and Henryk Dobslaw

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2024-641', Vagner Ferreira, 09 Apr 2024
  • RC2: 'Comment on egusphere-2024-641', Susanna Werth, 15 May 2024
  • RC3: 'Comment on egusphere-2024-641', Bramha Dutt Vishwakarma, 22 May 2024
Eva Boergens, Andreas Güntner, Mike Sips, Christian Schwatke, and Henryk Dobslaw
Eva Boergens, Andreas Güntner, Mike Sips, Christian Schwatke, and Henryk Dobslaw

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Short summary
The satellites GRACE and GRACE-FO observe continental terrestrial water storage changes. With over 20 years of data, we can look into long-term variations in the East Africa Rift region. We focus on whether the observed changes are due to natural variations or man-made. We found, both strong influences due to natural variability but also for Lake Victoria the influence of human actions. That is caused by the Nalubaale Dam, which regulates the outflow of Lake Victoria.